Yash Minerals & Minerals Properties Waraseoni, balaghat, Madhya Pradesh

Our company is a top Supplier of River Sand. We offer good quality River Sand at the most affordable price. Sand is a naturally occurring granular material composed of finely divided rock and mineral particles. The composition of sand is highly variable, depending on the local rock sources and conditions, but the most common constituent of sand in inland continental settings and non-tropical coastal settings is Silica (Silicon Dioxide, or SiO2), usually in the form of Quartz. The second most common form of sand is Calcium Carbonate, for example Aragonite, which has mostly been created, over the past half billion years, by various forms of life, like coral and shellfish. It is, for example, the primary form of sand apparent in areas where reefs have dominated the ecosystem for millions of years like the Caribbean.

We are one of the prominent Dolomite suppliers located in India. Dolomite Mineral is a sedimentary carbonate rock, consisting mainly of industrial of the mineral dolomite. Dolomite deposits are usually the land-use plan-associated with limestone. Dolomite has a number of uses, the most important of, which is construction, where it may be used as a substitute for limestone. Grades : Iron and Steel Industry : Dolomite is used in iron and steel industry as refractory raw materials and a flux. Ferro – Manganese : Contains MgO 19 to 20%, CaO 28 to 30%, SiO2 2 to 5% and R2O3 2 to 2.5%. Glass : For certain commercial glass, the Fe2O3 content up to 0.25% is permissible. For truly colorless glass Fe2O3 content of 0.04% (max.) is sometimes specification. Fertilizer Industry : Contains CaCO3 + MgCO3 90% (min.) and SiO2 5% max. Inferior grade dolomite limestone of 15 – 20% MgO can be used as soil conditioner. Lime : Contains CaCO3 58 – 75%, MgCO3 28-48% and other constituent should be less than 3%. Magnesium Metal : Contain MgO, 40.5%, CaO 58.10%, Fe2O3 0.8% and insoluble 0.6%. Chemical Formulae : CaMg(CO3)2 Usage : Substitute of lime stone Soil conditioner Achieves higher bulk density Refractory and Flux in industries Float glass production Applications : A soil conditioner Steel melting shop Refractory Detergents and soaps Flux Ink Iron and steel Powder coating Paint Ceramic industry Glass Construction Chemical Attributes : High degree of whiteness Hard Low moisture content Translucent Environment friendly Slow reaction with acids Lustrous High magnesium content High density

Bauxite is an aluminium ore and is the main source of aluminium. This form of rock consists mostly of the minerals gibbsite Al(OH)3, boehmite ?-AlO(OH), and diaspore a-AlO(OH), in a mixture with the two iron oxides goethite and hematite, the clay mineral kaolinite, and small amounts of anatase TiO2. Lateritic bauxites (silicate bauxites) are distinguished from karst bauxite ores (carbonate bauxites). The early discovered carbonate bauxites occur predominantly in Europe and Jamaica above carbonate rocks (limestone and dolomite), where they were formed by lateritic weathering and residual accumulation of intercalated clays or by clay dissolution residues of the limestone.

Quartz is the second most abundant mineral in the Earths continental crust, after feldspar. It is made up of a continuous framework of SiO4 silicon–oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall formula SiO2. There are many different varieties of quartz, several of which are semi-precious gemstones. Especially in Europe and the Middle East, varieties of quartz have been since antiquity the most commonly used minerals in the making of jewelry and hardstone carvings. The word quartz is derived from the German word Quarz and its Middle High German ancestor twarc, which probably originated in Slavic (cf. Czech tvrdy (hard), Polish twardy (hard)).

Iron is a chemical element with the symbol Fe (from Latin: ferrum) and atomic number 26. It is a metal in the first transition series. It is the most common element (by mass) forming the planet Earth as a whole, forming much of Earths outer and inner core. It is the fourth most common element in the Earths crust. Irons very common presence in rocky planets like Earth is due to its abundant production as a result of fusion in high-mass stars, where the production of nickel-56 (which decays to the most common isotope of iron) is the last nuclear fusion reaction that is exothermic.

We are known as one of the predominant Manganese Ore suppliers located in India. We supply the purest manganese ore mineral, from Balaghat, Malajkhand,Katni , Jabalpur,Chittisgadh (C.G) Maharastra (M.H) & All over India. Pure Manganese & All Minerals are available here

Iron is a chemical element with the symbol Fe (from Latin: ferrum) and atomic number 26. It is a metal in the first transition series. It is the most common element (by mass) forming the planet Earth as a whole, forming much of Earths outer and inner core. It is the fourth most common element in the Earths crust. Irons very common presence in rocky planets like Earth is due to its abundant production as a result of fusion in high-mass stars, where the production of nickel-56 (which decays to the most common isotope of iron) is the last nuclear fusion reaction that is exothermic. This causes radioactive nickel to become the last element to be produced before collapse of a supernova leads to the explosive events that scatter this precursor radionuclide of iron abundantly into space. Iron metal has been used since ancient times, though copper alloys, which have lower melting temperatures, were used first in history. Pure iron is soft (softer than aluminium), but is unobtainable by smelting.